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Table 2 Parameters of the inferred CMT solutions together with their uncertainty in terms of double standard deviation of Gaussian function (2σ) fitted to the respective marginal PDF

From: Bayesian inference and interpretation of centroid moment tensors of the 2016 Kumamoto earthquake sequence, Kyushu, Japan

No.

CMT location

DC component

DC component uncertainty

Lat.

Lon.

Depth (km)

M w

VR (%)

S/D/R (°)

DC (%)

S/D/R (°)

DC (%)

1

32.780

130.809

8.1

6.1

44

33/82/−155

64

3/7/9

± 24

2

32.696

130.768

3.8

6.0

58

212/77/178

87

2/9/12

± 20

3

32.862

130.856

8.4

5.7

59

294/37/−48

67

6/4/8

± 16

4

32.780

130.823

8.3

5.4

73

29/69/−149

94

2/3/4

± 10

5

32.765

130.760

13.0

5.0

45

6/72/−142

79

5/7/10

± 14

6

32.860

130.835

10.0

5.2

60

83/62/−71

89

3/2/3

± 10

7

32.692

130.716

7.8

5.2

74

68/63/−95

75

3/2/3

± 8

8

32.765

130.803

9.9

4.9

54

16/76/−163

92

2/4/4

± 14

9

32.679

130.735

8.1

4.9

71

211/66/175

90

2/3/3

± 8

10

32.745

130.752

5.7

4.7

53

215/81/−165

83

2/7/8

± 22

11

32.800

130.788

5.7

4.6

61

79/29/−104

98

8/2/8

± 12

  1. VR variance reduction, M w moment magnitude, S/D/R strike/dip/rake